Historical Reanalysis

ECMWF Reanalysis V5 (ERA 5) assimilates terrestrial- and space-based historical observations from January 1950 to present into a comprehensive, global gridded reanalysis dataset of past weather conditions. This is the ground truth dataset

The Salient forecast has a global extent and provides forecasts for latitude-longitude grid points at 0.25 x 0.25 degrees (25 km) resolution.

Update Frequency

Weekly on Thursday

Variables

The following is a list of nomenclature for variables, fields, dimensions, and models used in Salient's forecast and hindcast data files and API routes. The Variable name is used for API calls.

<aside> đź“Ś Hourly historical data is available for the following variables: temp, precip, rh, dhi, dni, tsi, cc, snow, sm, st, wgst, wdir, wspd, wspd100, wdir100.

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<aside> 📌 Note: The HDD | CDD calculations are slightly different from the traditional definition. Salient’s HDD/CDD calculation is the mean hourly difference by which the temperature subceeds/exceeds a temperature threshold (65F/18C) over the course of a day.  e.g. CDD = mean(floor(HourlyTemp-Threshold,0)) It is an hourly integral of temperature minus the base temperature. You can think of it as “mean degree-hours / day”.

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Name Variable Unit Description
Cloud Cover cc (0 - 1) Percentage of the sky hidden by all visible clouds.
Cooling Degree Days cdd °C °F
Diffuse Horizontal Irradiation dhi W/m² Diffuse horizontal irradiation is the part of the solar irradiation which has been scattered by the atmosphere that reaches a surface. Only available for hourly historical.
Direct Normal Irradiation dni W/m² Direct normal irradiation is the part of the solar irradiation that directly reaches a surface. Only available for hourly historical.
Evaporation evap mm/day Evaporation is the accumulated amount of water that has evaporated from the Earth's surface, including a simplified representation of transpiration (from vegetation), into vapor in the air above. Negative values indicate evaporation and positive values indicate condensation.
Heating Degree Days hdd °C °F
Geopotential Height (10 mbar) (250 mbar) (500 mbar) hgt10 hgt250 hgt500 m ft
Sea Level Pressure mslp mbar The sea level pressure is the atmospheric pressure at sea level at a given location.
Outgoing Longwave Radiation olr W/m² Longwave radiation directed (upwards) away from the surface
Precipitation precip mm/day Precipitation per day. To convert to an hourly rate (mm/hr), divide by 24.
Relative Humidity rh A dimensionless ratio, expressed in percent, of the amount of atmospheric moisture present relative to the amount that would be present if the air were saturated. Since the latter amount is dependent on temperature, relative humidity is a function of both moisture content and temperature. As such, relative humidity by itself does not directly indicate the actual amount of atmospheric moisture present.
Sea Ice Cover si (0 - 1)
Soil Moisture (upper 10 cm) sm m s**-1 The total amount of water, including the water vapor, in an unsaturated soil level (upper 10 cm).
Snow Cover snow m The areal extent of snow-covered ground.
Sea Surface Salinity sss psu Sea surface salinity describes the amount of salt in the water at the ocean surface.
Sea Surface Temperature sst °C °F
Soil Temperature (upper 10 cm) st °C °F
Temperature (2m) temp °C °F
Maximum Daily Temperature (2 m) tmax °C °F
Minimum Daily Temperature (2 m) tmin °C °F
Total Solar Insolation tsi W/m² The amount of solar radiation that reaches the earth’s surface over a period of time. It is equivalent to ghi, Global Horizontal Irradiation.
Wind Speed (10 m) (100 m)
wspd wspd100
m/s or mph The rate at which air is moving horizontally past a given point at 10m or 100m height above ground level
Wind Direction (10 m) (100 m)
wdir
wdir100 degrees The true direction from which the wind is blowing at a given location (i.e., wind blowing from the north to the south is a north wind) at 10m or 100m height. It is normally measured in tens of degrees from 10 degrees clockwise through 360 degrees. North is 360 degrees. A wind direction of 0 degrees is only used when wind is calm.
Wind Power (100m) wpow W/m² Wind power which is proportional to a density calculation and 100m wind speed cubed. The formula is 0.5 * air_density * sqrt (u² + v²)³, where u and v are the wind components and air_density is calculated at ground level and T = 15 °C.
Maximum Wind Gust (10 m) wgst m/s mph

Field

<aside> 📌 Hourly historical data is limited to “vals”.

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Name Variable
Anomaly anom
Detrended Anomaly anom_d
Standardized Detrended Anomaly anom_ds
Anomaly Quantiles anom_qnt
Standardized Anomaly anom_s
Climatology clim
Standard Deviation stdv
Trend trend
Value vals

v2/data_timeseries

https://api.salientpredictions.com/v2/documentation/api/#/Historical/get_data_timeseries